Décollement depth versus accretionary prism dimension in the Apennines and the Barbados

Author:

Bigi Sabina1,Lenci Federica1,Doglioni Carlo1,Moore J. Casey2,Carminati Eugenio1,Scrocca Davide3

Affiliation:

1. Dipartimento di Scienze della Terra; Università degli Studi di Roma “La Sapienza,”; Rome; Italy

2. Earth Sciences Department; University of California; Santa Cruz; California; USA

3. Istituto di Geologia Ambientale e Geoingegneria; Consiglio Nazionale delle Ricerche (CNR); Rome; Italy

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference75 articles.

1. Mineralogy and petrology of Grenada, Lesser Antilles island arc;Arculus;Contrib. Mineral. Petrol.,1978

2. Balanced sections and seismic reflection profiles across the central Apennines;Bally;Mem. Soc. Geol. It.,1986

3. Seismic velocities from the Barbados Ridge Complex: Indicators of high pore fluid pressures in an accretionary complex;Bangs;J. Geophys. Res.,1990

4. Lateral variation of seismic-wave attenuation in the upper mantle above the inclined earthquake zone of the Tonga Island arc: Deep anomaly the upper mantle;Barazangi;J. Geophys. Res.,1971

5. The CROP 03 profile: a synthesis of results on deep structures of the Northern Apennines;Barchi;Mem. Soc. Geol. It.,1998

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